Effect of orogeny, plate motion and land sea distribution on Eurasian climate change over the past 30 million years

被引：451

作者：

Ramstein, G ^{[1
]}

Fluteau, F ^{[1
]}

Besse, J ^{[1
]}

Joussaume, S ^{[1
]}

机构：

[1] UNIV PARIS 06,ORSTOM,CNRS,LAB OCEANOG DYNAM & CLIMATOL,F-75252 PARIS 05,FRANCE

来源：

NATURE | 1997年 / 386卷 / 6627期

关键词：

D O I：

10.1038/386788a0

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 [理学]; 0710 [生物学]; 09 [农学];

摘要：

The Eurasian climates of today, 10 million and 30 million years ago are simulated using an atmospheric general circulation model that incorporates realistic continental geography and epicontinental sea distributions. The resulting climates compare well with various palaeoclimate records. The retreat of the Paratethys-an epicontinental sea-shifts the central Asian climate from temperate to continental conditions, and plays as important a role as uplift, of the Himalayan/Tibetan plateau in driving the Asian monsoon changes.

引用

页码：788 / 795

页数：8

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